Another 60% came from changes to wind or ocean current patterns over the tropical Atlantic Ocean. The result was more warmed water reaching the southern East Coast and the Gulf.
“What makes it more complicated in Louisiana and Texas is the subsidence that comes on top of that, and that leads to rates of 14 to 15 millimeters a year,” Dangendorf said.
Warmer waters
Part of that natural variability, he said, is a 25- to 40-year cycle linked to lower and higher water temperatures in the Atlantic, called the Atlantic Multi-Decadal Oscillation.
Many climate scientists who study hurricanes believe that a warmer water version of that cycle began in 1995 and has stirred more frequent hurricanes.
The bright side of that finding is that sea-rise could slow back to the pre-2010 rate of 1.5 mm a year in about a decade.
Yet even that lower global rate, a mainstay since 1900, marked a significant increase in sea-level rise from the previous 3,000 years, the study found.
In his study, Yin discounted nearshore winds and changes in barometric pressure along coastlines as leading causes of the increase in sea level rise.
The loop
His research found another trend: more warm water feeding into the Gulf Stream and the Gulf of Mexico from a significant slowdown of a large, north-south oceanic pattern.
Yin argues that a downshift in the Atlantic Meridional Overturning Circulation, beginning in 2009 and 2010, injected even more warmth into the deep Loop Current, a segment of the Gulf Stream that breaks off every year or so and floats around the Gulf.
That bloated the size of water molecules, adding to sea level rise.
Yin also linked the acceleration to the heights of hurricane-induced storm surge in recent years.
He measured the surge and sea levels at local gauges from Texas to North Carolina over a half-dozen massive hurricanes: Harvey in 2017; Florence and Michael in 2018; Laura in 2020; Ida in 2021; Ian in 2022.
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